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Consistently dated records from the Greenland GRIP, GISP2 and NGRIP ice cores for the past 104 ka reveal regional millennial-scale δ18O gradients with possible Heinrich event imprint / Inger K. Seierstad; Peter M. Abbott; Matthias Bigler; Thomas Blunier; Anna J. Bourne; Edward Brook; Susanne L. Buchardt; Christo Buizert; Henrik B. Clausen; Eliza Cook; Dorthe Dahl-Jensen; Siwan M. Davies; Myriam Guillevic; Sigfús J. Johnsen; Desirée S. Pedersen; Trevor J. Popp; Sune O. Rasmussen; Jeffrey P. Severinghaus; Anders Svensson; Bo M. Vinther

Quaternary Science Reviews, Volume: 106, Pages: 29 - 46

Swansea University Author: Davies, Siwan

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DOI (Published version): 10.1016/j.quascirev.2014.10.032

Published in: Quaternary Science Reviews
Published: 2014
URI: https://cronfa.swan.ac.uk/Record/cronfa20722
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College: College of Science
Start Page: 29
End Page: 46